Clouds play a crucial role in regulating the Earth's climate by reflecting solar radiation, absorbing and trapping heat, and distributing water vapor through various atmospheric processes.

Stratus clouds are known for their uniform, gray appearance and typically cover the entire sky, often resulting in overcast conditions.

Condensation is the process where water vapor in the air cools and changes into liquid water droplets, leading to the formation of clouds.

Rain is the most common form of precipitation and consists of small, spherical water droplets that fall from clouds when the temperature is above freezing.

Coalescence is the process where smaller water droplets in clouds collide and merge with each other, resulting in the formation of larger droplets.

Cumulus clouds are characterized by their distinct puffy appearance and are commonly associated with fair weather conditions.

Sublimation is the process where water vapor in the air directly transforms into ice crystals without going through the liquid phase.

Sleet is a type of precipitation that occurs when raindrops freeze as they fall through a layer of cold air, resulting in small, round pellets of ice.

Deposition is the process where water vapor in the air directly condenses onto surfaces, bypassing the liquid phase, and forming tiny water droplets.

Cirrus clouds are characterized by their high altitude, thin, wispy appearance and are primarily composed of ice crystals.

Deposition is the process where water droplets in clouds directly freeze and become ice crystals, bypassing the liquid phase.

Hail is a type of precipitation that occurs when raindrops freeze as they fall through a layer of cold air, resulting in large, irregular-shaped pieces of ice.

Coalescence is the process where smaller ice crystals in clouds collide and merge with each other, resulting in the formation of larger ice crystals.

Altocumulus clouds are characterized by their layered, wavy appearance and are often associated with the approach of a warm front.

Melting is the process where ice crystals in clouds absorb heat and transition from a solid to a liquid state, becoming water droplets.